祁漫塔格肯德可克火山岩锆石LA-ICP-MS U-Pb、<sup>40</sup>Ar/<sup>39</sup>Ar年龄及地质意义

马帅; 陈世悦; 孙娇鹏; 汪峰; 单腾飞

祁漫塔格肯德可克火山岩锆石LA-ICP-MS U-Pb、⁴⁰Ar/³⁹Ar年龄及地质意义

1.
中国石油大学(华东)地球科学与技术学院, 山东青岛 266555
2.
西北大学大陆动力学国家重点实验室, 陕西西安 710069

基金项目:

中国地质调查局项目 [2014]03-025-002

详细信息

作者简介:
马帅(1990-), 男, 博士研究生, 研究方向为沉积学与盆地动力学.E-mail:mas0302@163.com

中图分类号: P597
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出版历程
- 收稿日期: 2016-12-31
- 刊出日期: 2017-08-01

A STUDY ON ZIRCON LA-ICP-MS U-PB AND ⁴⁰AR/³⁹AR AGES OF VOLCANIC ROCKS FROM KENDEKEKE, QIMANTAGE AND THE GEOLOGICAL SIGNIFICANCE

1.
College of Earth Science and Technology, China University of Petroleum, Qingdao 266555, Shandong, China
2.
State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, Shaanxi, China

摘要

摘要: 通过对采集到的肯德可克上泥盆统契盖苏群火山岩样品进行锆石LA-ICP-MS U-Pb测年和⁴⁰Ar/³⁹Ar定年，结合区域地质特征，本文对祁漫塔格构造带的多旋回构造演化进行了总结分析。研究表明，契盖苏群流纹岩形成于晚泥盆世（384.9±6.0 Ma），而契盖苏群的形成时间不晚于晚泥盆世。767±15 Ma、915±18 Ma两个继承性锆石年龄证明研究区响应了Rodinia超大陆聚合—裂解。地层、沉积、变质及变形等证据不支持祁漫塔格地区存在晚古生代洋盆或裂陷槽，晚古生代祁漫塔格地区是发育在柴达木西南缘的陆表海。样品⁴⁰Ar/³⁹Ar有效坪年龄为220.3±1.7 Ma，代表研究区最后一次埋深达约8000 m。晚三叠世火山活动之后，研究区发生大规模抬升，随后叠加了印支晚期、燕山、喜山等多期构造事件导致中新生代缺少大规模沉降。陆内造山持续到32 Ma左右，随后由于库木库里盆地的伸展，祁漫塔格造山带与东昆仑造山带分离。
- 肯德可克 /
- 火山岩 /
- 锆石U-Pb年龄 /
- Ar⁴⁰/Ar³⁹年龄 /
- 地质意义
Abstract: Zircon LA-ICP-MS U-Pb dating and ⁴⁰Ar/³⁹Ar dating were made on the volcanic samples of Qigaisu group from Kendekeke in upper Devonian. Combined with regional geological features, multicyclic tectonic evolution of Qimantag tectonic zone are summarized and analyzed. The results show that, rhyolites in Qigaisu group formed in late Devonian(384.9±6.0 Ma), while Qigaisu group formed no later than late Devonian. The two inherited zircon ages 767±15 Ma and 915±18 Ma certify that the study area responded to supercontinent aggregation-cracking, but evidence from stratum, sedimentation, metamorphism and deformation do not support the existence of the late Paleozoic ocean or aulacogen in Qimantag area, and Qimantag area in late Paleozoic was an epeiric sea located at the southwest margin of Qaidam. The ⁴⁰Ar/³⁹Ar effective plateau age of the samples is 220.3±1.7 Ma, which shows the latest burial depth is about 8000 m. Large-scale uplift events happened after the late Triassic volcanism, multiphase tectonic events, such as late Indosinian, Yanshanian and Himalayanian, caused the lack of large-scale settlement in Mesozoic and Cenozoic. Intra-continent orogeny lasted to 32 Ma or so. Because of the extension of Kumukuli basin afterwards, Qimantage orogenic belt separated from East Kunlun orogenic belt.
- Kendekeke /
- volcanic rock /
- zircon U-Pb age /
- ⁴⁰Ar/³⁹Ar age /
- geological significance

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图 1 肯德可克地区地质简图

Figure 1. Geological sketch of Kendekeke area

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图 2 测试样品QH-09-83流纹岩中的霏细结构

Figure 2. Felsitic texture in the rhyolite from testing sample QH-09-83

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图 3 肯德可克流纹岩的典型锆石阴极发光图像

Figure 3. CL images of typical zircons of rhyolites from Kendekeke area

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图 4 样品QH-09-83锆石U-Pb年龄谐和图

Figure 4. Zircon U-Pb concordia plot of sample QH-09-83

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图 5 样品QH-09-83⁴⁰Ar/³⁹Ar阶段升温年龄谱与等时线

Figure 5. ⁴⁰Ar/³⁹Ar stepwise incremental heating age spectra and isochron of sample QH-09-83

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表 1 样品QH-09-83锆石LA-ICPMS U-Pb测年结果表

Table 1. Zircon LA-ICPMS U-Pb dating results of sample QH-09-83

分析点	含量/×10^-6		U/Th	同位素比值						年龄/Ma
分析点	Th	U	U/Th	²⁰⁷Pb/ ²⁰⁶Pb	1σ	²⁰⁷Pb/ ²³⁵U	1σ	²⁰⁶Pb/ ²³⁸U	1σ	²⁰⁷Pb/ ²⁰⁶Pb	1σ	²⁰⁷Pb/ ²³⁵U	1σ	²⁰⁶Pb/ ²³⁸U	1σ
QH-09-83-01	140.6	180.0	1.28	0.0656	0.0025	0.6052	0.0180	0.0669	0.0014	793	77	481	11	418	9
QH-09-83-02	169.3	199.3	1.18	0.0557	0.0023	0.4843	0.0164	0.0631	0.0014	439	89	401	11	394	8
QH-09-83-03	173.2	311.6	1.80	0.0584	0.0021	0.5077	0.0138	0.0631	0.0013	544	75	417	9	394	8
QH-09-83-04	101.4	350.7	3.46	0.0925	0.0031	1.6114	0.0399	0.1263	0.0026	1478	62	975	16	767	15
QH-09-83-05	410.2	471.7	1.15	0.0607	0.0020	0.5124	0.0127	0.0612	0.0013	628	70	420	8	383	8
QH-09-83-06	277.0	318.2	1.15	0.0605	0.0021	0.4964	0.0131	0.0595	0.0012	622	73	409	9	373	8
QH-09-83-07	175.5	304.9	1.74	0.0558	0.0020	0.4524	0.0129	0.0588	0.0012	443	79	379	9	369	8
QH-09-83-08	139.0	186.4	1.34	0.0763	0.0031	0.6512	0.0213	0.0619	0.0014	1102	78	509	13	387	8
QH-09-83-09	233.6	362.3	1.55	0.0559	0.0019	0.4915	0.0125	0.0637	0.0013	450	74	406	9	398	8
QH-09-83-10	149.6	244.3	1.63	0.0589	0.0021	0.5096	0.0141	0.0628	0.0013	561	76	418	9	393	8
QH-09-83-11	207.1	324.2	1.57	0.0817	0.0028	0.7106	0.0189	0.0631	0.0013	1237	67	545	11	395	8
QH-09-83-12	214.8	351.3	1.64	0.0618	0.0022	0.5399	0.0146	0.0633	0.0013	669	73	438	10	396	8
QH-09-83-13	212.0	256.0	1.21	0.0610	0.0021	0.5292	0.0142	0.0629	0.0013	641	73	431	9	393	8
QH-09-83-14	105.0	163.0	1.55	0.0798	0.0028	0.6822	0.0188	0.0620	0.0013	1192	69	528	11	388	8
QH-09-83-15	265.8	394.6	1.48	0.0542	0.0019	0.4626	0.0122	0.0620	0.0013	377	76	386	8	388	8
QH-09-83-16	110.5	184.9	1.67	0.0582	0.0022	0.4974	0.0146	0.0620	0.0013	538	79	410	10	388	8
QH-09-83-17	279.6	354.1	1.27	0.1292	0.0045	1.1017	0.0295	0.0619	0.0013	2086	60	754	14	387	8
QH-09-83-18	140.9	220.5	1.57	0.0566	0.0021	0.4842	0.0139	0.0621	0.0013	474	79	401	10	388	8
QH-09-83-19	139.6	234.2	1.68	0.0537	0.0021	0.4673	0.0145	0.0631	0.0014	357	84	389	10	395	8
QH-09-83-20	110.5	206.8	1.87	0.0564	0.0024	0.4497	0.0161	0.0578	0.0013	468	92	377	11	362	8
QH-09-83-21	123.0	183.5	1.49	0.0618	0.0025	0.5221	0.0173	0.0613	0.0013	667	83	427	12	383	8
QH-09-83-23	102.9	170.7	1.66	0.0542	0.0022	0.4533	0.0155	0.0607	0.0013	378	89	380	11	380	8
QH-09-83-24	153.3	254.8	1.66	0.0547	0.0020	0.4936	0.0145	0.0654	0.0014	401	80	407	10	408	8
QH-09-83-25	258.5	384.2	1.49	0.0585	0.0021	0.4982	0.0143	0.0618	0.0013	547	77	411	10	387	8
QH-09-83-26	159.2	240.8	1.51	0.0684	0.0024	1.4374	0.0404	0.1524	0.0033	880	72	905	17	915	18
QH-09-83-27	182.2	312.5	1.72	0.0554	0.0022	0.4463	0.0142	0.0584	0.0013	429	84	375	10	366	8
QH-09-83-28	842.7	1052.5	1.25	0.0730	0.0026	0.5386	0.0152	0.0535	0.0011	1015	71	438	10	336	7
QH-09-83-29	332.5	438.4	1.32	0.0550	0.0021	0.4715	0.0143	0.0622	0.0013	412	81	392	10	389	8
QH-09-83-30	288.6	398.1	1.38	0.0550	0.0021	0.4962	0.0150	0.0654	0.0014	412	81	409	10	409	9

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表 2 样品QH-09-83钾长石⁴⁰Ar/³⁹Ar阶段升温分析结果

Table 2. ⁴⁰Ar/³⁹Ar stepwise incremental heating results of potash feldspar in sample QH-09-83

T/℃	(⁴⁰Ar/³⁹Ar)_m	(³⁶Ar/ ³⁹Ar) _m	(³⁷Ar/ ³⁹Ar) _m	(³⁸Ar/ ³⁹Ar) _m	⁴⁰Ar/%	F	³⁹Ar/×10 ^-14mol	³⁹Ar(Cum.)/%	Age/Ma	±1 s/Ma
700	56.1874	0.1349	0	0.0407	29.02	16.3067	0.37	0.95	245.5	3.1
800	22.208	0.0234	0.0671	0.0172	68.88	15.298	8.99	24.11	231.2	2.2
850	15.8355	0.0031	0	0.0128	94.14	14.9069	6.19	40.07	225.6	2.1
900	15.6058	0.0036	0.0057	0.0131	93.18	14.5409	5.89	55.26	220.4	2.1
950	15.7663	0.0047	0	0.0135	91.13	14.3677	5.01	68.18	218	2.1
1000	16.2629	0.0064	0.0259	0.0141	88.43	14.3816	4.98	81.02	218.2	2.1
1050	16.9776	0.0081	0	0.0144	85.87	14.5794	2.13	86.52	221	2.1
1120	17.0973	0.0085	0.0311	0.0143	85.36	14.5953	2.43	92.79	221.2	2.1
1200	16.1227	0.0047	0.0169	0.014	91.45	14.7438	1.89	97.68	223.3	2.2
1280	17.8253	0.0068	0	0.0141	88.76	15.8225	0.42	98.77	238.6	4.7
1400	55.0893	0.0239	0.8873	0.0234	87.27	48.1131	0.48	100	645.3	5.8

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